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Chapter 3. Applications of the Basic Equations 3.1 Isobaric Coordinates. Horizontal Momentum Equation. Total Derivative. Geostrophic Relations. 3.1.2 Continuity Equation In Isobaric Coordinate System. 3.2 Balanced Flow. Several Types of Balanced Flow. n. ds. s(x,y,t). t. stream- lines.
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Chapter 3. Applications of the Basic Equations3.1 Isobaric Coordinates Reinisch_85.515
Horizontal Momentum Equation Reinisch_85.515
Total Derivative Reinisch_85.515
Geostrophic Relations Reinisch_85.515
3.1.2 Continuity EquationIn Isobaric Coordinate System Reinisch_85.515
3.2 Balanced Flow Reinisch_85.515
Several Types of Balanced Flow Reinisch_85.515
n ds s(x,y,t) t stream- lines 3.2.1 Natural Coordinate System Reinisch_85.515
change of speed along s centripetal acceleration Acceleration in Natural Coordinates Reinisch_85.515
Coriolis Force in Natural Coordinates Reinisch_85.515
FPG Vg F=F0-dF FCo F=F0 3.2.2 Geostrophic Flow Reinisch_85.515
3.2.3 “Inertial” Flow (F=const) Reinisch_85.515
Period of Inertial Oscillation Reinisch_85.515
3.2.4 Cyclostrophic Flow (Fco 0) Reinisch_85.515
Tornado, An Example Of Cyclostrophic Flow Reinisch_85.515
3.2.5 Gradient Wind( ) Reinisch_85.515
Speed of the Gradient Wind Reinisch_85.515
3.3 Trajectories and Streamlines Reinisch_85.515
Radius of Curvature Reinisch_85.515
3.4 The Thermal Wind Reinisch_85.515
Vertical Wind Shear Reinisch_85.515
Vertical Wind Shear Reinisch_85.515